A State Rarity Rank of S3 means: Typically 21 to 100 occurrences, limited acreage, or miles of stream in New York State.

Global Rarity Rank:G4

A Global Rarity Rank of G4 means: Apparently secure globally, though it may be quite rare in parts of its range, especially at the periphery.

Did you know?
Unlike most terrestrial systems, maritime dune systems move over the landscape and even across property boundaries. Consequently, this migrating dune system is difficult to preserve. However, it needs to be protected and restored. A healthy dune system protects property by reducing the energy of storm waves. It is the best defense against coastal flooding, erosion, and sea-level rise. It provides tremendous economic benefit to the local economy. A healthy coastal sand dune system is also the least costly way to maintain a recreational beach for future generations. (http://www.maine.gov/dep/blwq/topic/dunes/)

There are an estimated 130 miles of maritime dunes on Long Island (about 100 miles on the south shore) covering about 4,700 to 14,000 acres; there may be as many as 30 to 50 extant occurrences statewide. The several documented occurrences have good viability and most are protected on public or private conservation land. This community is restricted to the ocean shoreline of southern and eastern Long Island and includes some high quality examples. The trend for the community is declining due to threats related to alteration of dune/swale dynamics, including management practices that alter natural hydrologic processes (such as breach contingency plans), dune fragmentation, loss of connectivity between the open ocean and the uplands, ORV use, and coastal development.

Although the number of maritime dunes may have increased slightly when formerly long, continuous examples were fragmented by development, the acreage of maritime dunes in New York has probably declined in recent decades as a result of coastal development and recreational overuse. Community viability/ecological integrity is suspected to be slowly declining, primarily due to anthropogenic alterations (both physical and hydrological) to dune and swale dynamics and coastal development (e.g., fragmentation, shoreline hardening, filling, road construction, and community destruction).

Although the number of maritime dunes in New York may have increased substantially from historical numbers when formerly long, continuous examples were fragmented by development into numerous large and small stretches of dunes, their aerial extent and viability are suspected to have declined substantially over the long-term. These declines are likely correlated with coastal development and associated changes in connectivity, hydrology, water quality, and natural processes.